Long-term effect of the Kärdla crater (Hiiumaa, Estonia) on Late Ordovician carbonate sedimentation

Author:

Ainsaar Leho,Suuroja Kalle,Semidor Maili

Publisher

Elsevier BV

Subject

Oceanography

Reference27 articles.

1. Ainsaar, L., Kirsimäe, K., Meidla, T., 1996. Regression in Caradoc: evidences from southwestern Estonia (Ristiküla core). In: Stouge, S. (Ed.), WOGOGOB-94 Symposium. Working Group of Ordovician Geology of Baltoscandia, Bornholm-94. Geological Survey of Denmark and Greenland Report 98, pp. 5–12.

2. The pattern of global bio-events during the Ordovician period;Barnes,1995

3. Discontinuity surfaces of possible microkarst origin in the Viivikonna Formation (Kukruse stage, Middle Ordovician) of Estonia. Proceedings of the Academy of Sciences of the Estonian SSR;Bauert;Geology,1989

4. Cooper, R.A., 1999. The Ordovician time scale—calibration of graptolite and conodont zones. In: Kraft, P., Fatka, O. (Eds.), Quo vadis Ordovician? Acta Universitatis Carolinae Geologica 43, 1–4.

5. Precise chitinozoan dating of impact events in Baltoscandia;Grahn;Journal of Micropalaeontology,1996

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